• The Core Journal of China
  • Included in Chinese Science Citation Database
  • The Key Magazine of China technology
  • Frontrunner 5000—Top Articles in Outstanding S&T Journals of China
  • Included in Scopus
  • Included in Chemical Abstracts (CA)
  • Included in Russian Abstract Journal (AJ)
Advanced Search
SONG Teng, LIN Tuo, LI Fei, LI Haohan, WU Hai, DUAN Ke. Lithofacies paleogeography in the depositional period of the Datangpo Formation of Nanhua System in the Middle and Upper Yangtze Region, SW China and its indication of hydrocarbon accumulation[J]. GEOLOGY IN CHINA.
Citation: SONG Teng, LIN Tuo, LI Fei, LI Haohan, WU Hai, DUAN Ke. Lithofacies paleogeography in the depositional period of the Datangpo Formation of Nanhua System in the Middle and Upper Yangtze Region, SW China and its indication of hydrocarbon accumulation[J]. GEOLOGY IN CHINA.

Lithofacies paleogeography in the depositional period of the Datangpo Formation of Nanhua System in the Middle and Upper Yangtze Region, SW China and its indication of hydrocarbon accumulation

Funds: 

Supported by the project of China Geological Survey (No.DD20190088)

More Information
  • Available Online: February 03, 2024
  • [Objective]Marine black manganese-bearing carbonaceous shale of Datangpo Formation was generally developed in the mid-Neoproterozoic Nanhua period in the Middle-Upper Yangtze Region, South China, which has been widely concerned as a manganese deposit for a long time, but with little attention to its petroleum geological characteristics. This paper expounds the lithofacies paleogeography of the Datangpo Formation and its indication of oil and gas accumulation, so as to guide the oil and gas investigation in the Suthern China.[Methods] Through field investigation and data collection on the Datangpo Formation, the oil and gas geological conditions, the source rock characteristics and hydrocarbon accumulation assemblage, especially lithofacies and paleogeography, were systematically analyzed by methods of single well analysis, continuous well comparison, lithofacies paleogeographic map compilation, etc., combined with source rock characteristic analysis, reservoir analysis and other experimental testing methods.[Results] The Datangpo Formation was formed during the interglacial period, and the depositional process was controlled by the extensional rifting process. Its sedimentary facies can be divided into two types, seven subtypes and several microfacies. The entire depositional period constitutes a complete transgressive-Highstand-Regressive sedimentary cycle; the most potential facies belts for oil and gas resources in the Datangpo Formation are limited shelf subfacies and lagoon subfacies, mainly distributed in the first member, with good organic geochemical index characteristics, and are high-quality source rocks.[Conclusions] The first member of the Datangpo Formation has good hydrocarbon generation and shale gas development potential. Songtao, Huayuan, Xiushan, Xiangtan, Hefeng and other areas at the junction of Hunan, Chongqing and Guizhou Province have favorable conditions for shale gas development and are potential shale gas development areas. With the Datangpo Formation as the source rock, a variety of potential reservoir-forming assemblages can be formed. The Xiushan, Songtao and Huayuan areas at the junction of Chongqing, Guizhou and Hunan Province have good source-reservoir configuration conditions and are potential conventional oil and gas development areas.
  • Related Articles

    [1]SONG Teng, LIN Tuo, LI Fei, LI Haohan, WU Hai, DUAN Ke. Lithofacies paleogeography during the depositional period of the Nanhua System Datangpo Formation and its indications for hydrocarbon accumulation in the Middle and Upper Yangtze Region, South China[J]. GEOLOGY IN CHINA. DOI: 10.12029/gc20210602004
    [2]QIN Yong. Thinking and discussion for some problems of geological survey of coal measures gas[J]. GEOLOGY IN CHINA, 2023, 50(5): 1355-1374. DOI: 10.12029/gc20230222001
    [3]ZHANG Yuxuan, TANG Jinrong, NIU Yazhuo, ZHANG Jingya, ZHAO Yu, WEI Jianshe, JIANG Guangzheng, WANG Liwei. Resource advantage and geological work suggestions under carbon neutralization in Northwest China[J]. GEOLOGY IN CHINA, 2022, 49(5): 1458-1480. DOI: 10.12029/gc20220507
    [4]XIA Riyuan, LU Haiping, CAO Jianwen, ZHAO Liangjie, WANG Zhe, LUAN Song. Characteristics of groundwater resources of karst areas in the Southern China and water resources guarantee countermeasures[J]. GEOLOGY IN CHINA, 2022, 49(4): 1139-1153. DOI: 10.12029/gc20220408
    [5]LIN Tuo, YUAN Kun, CHEN Xianglin, WANG Shengjian, JIN Chunshuang, WANG Chao. Industrial gas flow of Carboniferous shales in southern China was obtained in Well Qianshuidi 1 in Guizhou Province[J]. GEOLOGY IN CHINA, 2022, 49(3): 995-996. DOI: 10.12029/gc20220323
    [6]YANG Yuru, MENG Fanyang, BAI Minggang, ZHANG Jiazheng, XIA Xianghua, BAO Shujing, HU Zhifang, ZHANG Cong, WANG Yufang, SONG Teng, WANG Xianghua, YU Weixin. An analysis of reservoir characteristics, resources and exploration prospects of the oldest shale gas in the world[J]. GEOLOGY IN CHINA, 2020, 47(1): 14-28. DOI: 10.12029/gc20200102
    [7]LI Wen-hao, ZHANG Zhi-huan, LI You-chuan, ZHANG Gong-cheng, FU Ning. The development characteristics of source rocks in the main deepwater petroliferous basins of the world and their enlightenment to the study of source rocks in deep-water area of northern South China Sea[J]. GEOLOGY IN CHINA, 2014, 41(5): 1673-1681. DOI: 10.12029/gc20140521
    [8]CHENG Zhi-zhong, XIE Xue-jing, PAN Han-jiang, YANG Rong. Geological characteristics of Te anomalies in South China[J]. GEOLOGY IN CHINA, 2012, 39(2): 295-301. DOI: 10.12029/gc20120203
    [9]Toshiaki ITO, Fumio KANAI, Kazuro BANDO, Research group for arsenic contamination of groundwater in Inner Mongolia, Asia Arsenic Network, Research Group for Applied Geology. 中国内蒙古河套[J]. GEOLOGY IN CHINA, 2010, 37(3): 730-740. DOI: 10.12029/gc20100327
    [10]DAI Jin-xing, WEI Yan-zao, ZHAO Jing-zhou. Important role of the formation of gas accumulations in the late stage in the formation of large gas fields[J]. GEOLOGY IN CHINA, 2003, 30(1): 10-19. DOI: 10.12029/gc20030102

Catalog

    Article views (8054) PDF downloads (762) Cited by()

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return